Book contents
- Frontmatter
- TO THE READER
- Contents
- LIST OF WOOD-CUTS
- STROMNESS AND ITS ASTEROLEPIS.—THE LAKE OF STENNIS
- THE DEVELOPMENT HYPOTHESIS, AND ITS CONSEQUENCES
- THE RECENT HISTORY OF THE ASTEROLEPIS.—ITS FAMILY
- CEREBRAL DEVELOPMENT OF THE EARLIER VERTEBRATA.—ITS APPARENT PRINCIPLE
- THE ASTEROLEPIS.—ITS STRUCTURE, BULK, AND ASPECT
- FISHES OF THE SILURIAN ROCKS, UPPER AND LOWER.—THEIR RECENT HISTORY, ORDER, AND SIZE
- HIGH STANDING OF THE PLACOIDS.—OBJECTIONS CONSIDERED
- THE PLACOID BRAIN.—EMBRYOTIC CHARACTERISTICS NOT NECESSARILY OF A LOW ORDER
- THE PROGRESS OF DEGRADATION.—ITS HISTORY
- EVIDENCE OF THE SILURIAN MOLLUSCS.—OF THE FOSSIL FLORA.—ANCIENT TREE
- SUPERPOSITION NOT PARENTAL RELATION.—THE BEGINNINGS OF LIFE
- LAMARCKIAN HYPOTHESIS OF THE ORIGIN OF PLANTS.—ITS CONSEQUENCES
- THE TWO FLORAS, MARINE AND TERRESTRIAL.—BEARING OF THE EXPERIENCE ARGUMENT
- THE DEVELOPMENT HYPOTHESIS IN ITS EMBRYOTIC STATE.—OLDER THAN ITS ALLEGED FOUNDATIONS
- FINAL CAUSES.—THEIR BEARING ON GEOLOGIC HISTORY.—CONCLUSION
STROMNESS AND ITS ASTEROLEPIS.—THE LAKE OF STENNIS
Published online by Cambridge University Press: 29 August 2010
- Frontmatter
- TO THE READER
- Contents
- LIST OF WOOD-CUTS
- STROMNESS AND ITS ASTEROLEPIS.—THE LAKE OF STENNIS
- THE DEVELOPMENT HYPOTHESIS, AND ITS CONSEQUENCES
- THE RECENT HISTORY OF THE ASTEROLEPIS.—ITS FAMILY
- CEREBRAL DEVELOPMENT OF THE EARLIER VERTEBRATA.—ITS APPARENT PRINCIPLE
- THE ASTEROLEPIS.—ITS STRUCTURE, BULK, AND ASPECT
- FISHES OF THE SILURIAN ROCKS, UPPER AND LOWER.—THEIR RECENT HISTORY, ORDER, AND SIZE
- HIGH STANDING OF THE PLACOIDS.—OBJECTIONS CONSIDERED
- THE PLACOID BRAIN.—EMBRYOTIC CHARACTERISTICS NOT NECESSARILY OF A LOW ORDER
- THE PROGRESS OF DEGRADATION.—ITS HISTORY
- EVIDENCE OF THE SILURIAN MOLLUSCS.—OF THE FOSSIL FLORA.—ANCIENT TREE
- SUPERPOSITION NOT PARENTAL RELATION.—THE BEGINNINGS OF LIFE
- LAMARCKIAN HYPOTHESIS OF THE ORIGIN OF PLANTS.—ITS CONSEQUENCES
- THE TWO FLORAS, MARINE AND TERRESTRIAL.—BEARING OF THE EXPERIENCE ARGUMENT
- THE DEVELOPMENT HYPOTHESIS IN ITS EMBRYOTIC STATE.—OLDER THAN ITS ALLEGED FOUNDATIONS
- FINAL CAUSES.—THEIR BEARING ON GEOLOGIC HISTORY.—CONCLUSION
Summary
When engaged in prosecuting the self-imposed task of examining in detail the various fossiliferous deposits of Scotland, in the hope of ultimately acquainting myself with them all, I extended my exploratory ramble, about two years ago, into the Mainland of Orkney, and resided for some time in the vicinity of Stromness.
This busy seaport town forms that special centre, in this northern archipelago, from which the structure of the entire group can be most advantageously studied. The geology of the Orkneys, like that of Caithness, owes its chief interest to the immense development which it exhibits of one formation,—the Lower Old Red Sandstone,—and to the extraordinary abundance of its vertebrate remains. It is not too much to affirm, that in the comparatively small portion which this cluster of islands contains of the third part of a system regarded only a few years ago as the least fossiliferous in the geologic scale, there are more fossil fish enclosed than in every other geologic system in England, Scotland, and Wales, from the Coal Measures to the Chalk inclusive. Orkney is emphatically to the geologist what a juvenile Shetland poetess designates her country, in challenging for it a standing independent of the “Land of Cakes,”—a “Land of Fish;” and, were the trade once fairly opened up, could supply with ichthyolites, by the ton and the shipload, the museums of the world.
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- Footprints of the CreatorOr, the Asterolepis of Stromness, pp. 1 - 12Publisher: Cambridge University PressPrint publication year: 2009First published in: 1849